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To ensure only tightly correlated probes were clustered, we employed a stringent cutoff (correlation distance cutoff 0.2).
Fig. 4 Correlation distance at the seismic stations.
The shorter the correlation distance is, the higher the observed attenuation is due to heterogeneities.
Model M uses the declustered moderate-size earthquake catalog and a correlation distance of 75 km.
This is modelled through a process with a lognormal distribution and a correlation distance.
The shorter the correlation distance is, the smaller value the B theo. marks.
where x0 is correlation distance of local mean power and xav is smoothing window length.
The vertical correlation distance was set to 1 km, without significant vertical smearing.
Clustering in the heat maps is based on average linkage method and Pearson correlation distance metric.
We use a correlation distance of 50 km for the smoothing.
The observed B values also showed similar distribution to that of the correlation distance.
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